Consistency of recently observed trends over the Baltic Sea basin with climate change projections

7th Study Conference on BALTEX

10-14 June 2013, Sweden

Hans von Storch, Armineh Barkhordarian, Juan J. Gómez-Navarro

2

Introduction

In this study we investigate the consistency of observed trends with climate

change projections.

The principle aim of “consistency” method is to tackle the question, whether the

recent change is a plausible harbinger of future change that is, we examine to

what extent the observed climate trends are already an indication of the

conditions described by the climate change scenarios (A1B) at the end of this

century.

Jonas Bhend and Hans von Storch (2008) Consistency of observed winter precipitation trends in

northern Europe with regional climate change projections. 31,17-28.

Jonas Bhend and Hans von Storch (2009) Is greenhouse gas forcing a plausible explanation for the

observed warming in the Baltic Sea catchment area? Boreal Environment Research. 14, p81.

3

Data

Parameters and observed datasets used: 2m Temperature CRUT Precipitation CRU, GPCC6, GPCP Mean Sea-level pressure HadSLP2 500 hPa Geopotental height NCEP/NCAR Specific and relative humidity HadCRUH Cloud cover CRU Surface solar radiation MFG Satellites

Models: 10 simulations of RCMs are used from ENSEMBLES project

Estimating natural variability: 2,000-year high-resolution regional climate Palaeosimulation is used to estimate natural

(internal+external) variability.

(Gómez-Navarro, J. J., Montávez, J. P., Wagner, S., and Zorita, E.: A regional climate palaeosimulation for

Europe in the period 1500–1990 – Part 1: Model validation, Clim. Past Discuss., 9, 1803-1839, 2013)

4

2m Temperature (1980-2009)

MAM JJA SON Annual

Observed trends in 1980-2009

Projected GS signal, A1B scenario

10 simulations, ENSEMBLES

95th-%tile of „non-GHG“ variability,

derived from 2,000-year palaeo-simulations

The spread of trends of 10 RCM simulations

GHG forcing allows for reconstructing the recently observed warming over the Baltic Sea

area (with less than 5% risk of error) None of the 10 regional climate projections capture the observed warming, which is

pronounced in winter (DJF).

Observed changes of 2m Temperature

(1980-2009) in comparision with GS signal

5

2m-Temperature (1930-2009)

Seasonal regression indices of observed

moving 30-year trends based on CRUT onto

the multi-model mean GS (Greenhouse gas

and Sulfate aerosols) signal. The gray

shaded area indicates the 95% uncertainty

range of regression indices, derived from fits

of the regression model to 2,000-year

palaeo-simulations.

Seasonal Regression Indices

In winter (DJF), summer (JJA) and autumn

(SON) the gray shaded areas exclude zero line

but include unit scaling for 30-year trends

ending in 2000 and later, indicating the

emergence of a detectable GS influence (with

less than 5% risk of error).

6

Precipitation (1979-2008)

Observed (CRU3, GPCC6, GPCP)

Projected GS signal (ENSEMBLES)

In winter (DJF) non of the 59

segments derived from 2,000 year

palaeo-simulations yield a positive

trend of precipitation as strong as that

observed. There is less than 5%

probability that observed positive

trends in winter be due to natural

(internal + external) variability alone

(with less than 5% risk).

In spring (MAM), summer (JJA) and Annual trends externally forced changes are not detectable. However

observed trends lie within the range of changes described by 10 climate change scenarios, indicating that

also in the scenarios a systematic trend reflecting external forcing is not detectable (< 5% risk).

In autumn (SON) the observed negative trends of precipitation contradicts the upward trends suggested by

10 climate change scenarios, irrespective of the observed dataset used.

7

Winter-time precipitation (1930-2009)

Regression indices of

Winter-time precipitation (1930-2009)

End of moving 40-year trends

Regression indices of observed moving

40-year trends of precipitation in DJF onto

the multi-model mean GS signal. The gray

shaded area indicates the 95% uncertainty

range of regression indices, derived from

fits of the regression model to 2,000-year

palaeo-simulations.

The gray shaded area exclude the zero line

but includes unit scaling for 40-year trends

ending in 1995 and later, indicating the

concerted emergence of the GS signal in the

late 20th and 21st century.

Obtained results are insensitive to the

removal of NAO fingerprint

1

8

Precipitation (1979-2008)

We further examine the possibility that the

inconsistency of observed precipitation trends

in autumn (SON) with regional climate change

projections may be related to trends in large-

scale circulations.

10

Changes in Large-scale circulation (SON)

Observed trend pattern shows areas of decrease in SLP over the Med. Sea and areas

of increase in SLP over the northern Europe. Observed trend pattern of SLP in SON

contradicts regional climate projections.

The mismatch between projected and observed precipitation in autumn is already

present in the atmospheric circulation.

Mean Sea-level pressure (SON)

Projected GS signal

pattern (RCMs)

Observed trend pattern

(1978-2009)

11

Summary Table 1

12

Summary Table 2

YES

13

Conclusions

Temperature:• Anthropogenic (Greenhouse gas and Sulfate aerosols, GS) forcing has a detectable influence

in the recently observed seasonal and annual warming trends over the Baltic Sea area.• However, in terms of magnitude of change, regional climate change projections underestimate

the observed warming.

Precipitation:

• The influence of GS signal is detectable in winter-time precipitation. However, in autumn

observed negative trends contradicts the upward trends projected by 10 regional climate

change projections, irrespective of the observed datasets used.

• Obtained results are insensitive to the removal of NAO fingerprint.

• The analysis of large-scale circulation patterns, in terms of mean sea-level pressure and

geopotential height at 500 hPa, confirms the inconsistency detected for precipitation in autumn.

Surface Humidity:• Observation show an upward trend in surface specific humidity in all seasons. In summer the

increase in specific humidity is very unlikely due to natural (internal+external) variability alone.

• In contrast, relative humidity remains approximately constant, which is consistent with climate change projections.

Similar analysis for Mediterranean region (see publications Barkhordarian et al) - with similar

results, including the inconsistency in SON, but this time more precip in the past with expected

reduction.